Taxonomy
-Syntype 1 illustrated below should be declared a lectotype. [copied from Chronos database]
Original description: "Test large, strongly spiroconvex, coiled in a high trochospire. Spiral side strongly convex, umbilical side convex. Equatorial periphery circular, slightly lobate with a double keel composed of one primary and strongly beaded keel and a weakly developed secondary keel visible in the umbilical side of the periphery. Chambers arranged in 4 whorls increasing in size in the direction of coiling. Initial chambers small and globular and followed by larger, subpetaloid chambers becoming gradually larger in the direction of coiling. Final whorl composed of subpetaloid chambers on spiral side, on umbilical side ovoid chambers elongated in the direction of coiling. Sutures on spiral side curved, raised and strongly beaded, on umbilical side slightly curved, raised in the beginning of the last whorl and finally become depressed. Umbilicus raised in the beginning of the last whorl and finally become depressed. Umbilicus wide and deep, surrounded by periumbilical ridges and covered by tegilla. Primary aperture interiomarginal umbilical. Accessory apertures intralaminal. Surface smooth. Wall calcareous, perforate except for tegilla and keels."
Entries in the Catalog of original descriptions: Globotruncana conica, Globotruncana dorreeni
Character matrix
| test outline: | Circular | chamber arrangement: | Trochospiral | edge view: | Spiroconvex | aperture: | Umbilical |
| sp chamber shape: | Subrectangular | coiling axis: | Moderate-high | periphery: | Single keel | aperture border: | Thin porticus |
| umb chbr shape: | Trapezoidal | umbilicus: | Wide | periph margin shape: | Subangular | accessory apertures: | Intralaminal |
| spiral sutures: | Raised beaded | umb depth: | Deep | wall texture: | Finely pustulose | shell porosity: | |
| umbilical or test sutures: | Weakly depressed | final-whorl chambers: | 6-9 | N.B. These characters are used for advanced search. N/A - not applicable | |||
Geological Range:
Last occurrence (top): within G. gansseri zone (71.73-73.80Ma, top in Maastrichtian stage). Data source: [copied from Chronos database]
First occurrence (base): within G. gansseri zone (71.73-73.80Ma, base in Campanian stage). Data source: [copied from Chronos database]
Plot of range and occurrence data:
Almogi-Labin, A., Reiss, Z & Caron, M. (1986). Senonian globotruncanidae from Israel. Eclogae Geologicae Helvetiae. 79(3): 849-895. gs O Pessagno, E. A. (1967). Upper Cretaceous planktonic foraminifera from the western Gulf Coastal Plain. Palaeontographica Americana. 5: 245-445. gs O Postuma, J. A. (1971). Manual of planktonic foraminifera. Elsevier for Shell Group, The Hague. 1-406. gs Smith, C. C. & Pessagno, E. A. (1973). Planktonic foraminifera and stratigraphy of the Corsicana formation (Maestrichtian) North-central Texas. Cushman Foundation for Foraminiferal Research, Special Publication. 12: 1-67. gs O White, M. P. (1928). Some Index Foraminifera of the Tampico Embayment Area of Mexico. Journal of Paleontology. 2(3): 177-215. gs References:

![]()
![]() |
Globotruncanita conica compiled by the pforams@mikrotax project team viewed: 13-10-2026
Short stable page link: https://mikrotax.org/pforams/index.php?id=110192 Go to Archive.is to create a permanent copy of this page - citation notes |
This policy contains information about your privacy. By posting, you are declaring that you understand this policy:
This policy is subject to change at any time and without notice.
These terms and conditions contain rules about posting comments. By submitting a comment, you are declaring that you agree with these rules:
Failure to comply with these rules may result in being banned from submitting further comments.
These terms and conditions are subject to change at any time and without notice.
Comments