Taxonomy
Original description: Test broad and rounded, about 1½ times as broad, initial portion rapidly tapering, later portion of nearly uniform width, periphery of early portion keeled, later indented; chambers of the early portion somewhat compressed, keeled, much broader than high, rapidly inflated in the adult where they are globular; sutures in the early portion slightly costate or with the fine perforations in vertical lines, in the adult thicker-walled with the surface rather coarsely punctate; aperture, a low, broad arch with a slight lip, the sides continuing in flange onto the preceding chamber.
Entries in the Catalog of original descriptions: Guembelina punctulata, Pseudotextularia echevarriai, Heterohelix (Heterohelix) planeobtusa, Heterohelix robusta
Emended description: Georgescu. 2007, p.6: "Test biserial throughout at most specimens, consisting of ten to seventeen chambers. Chamber proliferation may occur between the two rows of diverging chambers. Chambers are subspherical throughout, distinctly overlapping the previous ones these resulting in a slightly lobate test periphery in lateral view. They increase rapidly in size in the earlier part of the test but more slowly in the adult portion. Sutures are distinct, depressed, and straight to slightly oblique to the growth axis. Periphery broadly rounded, without peripheral structures such as rows of pustules, keels, etc. Aperture is situated at the base of the last formed chamber and is bordered by a wide, imperforate band. Test with irregularly reticulate ornamentation throughout; occasionally the last-formed chambers are longitudinally costate. Test wall is calcareous, hyaline, and finely perforate, pore diameter fluctuating between 1.3 and 2.4 microns. The size of the pores is dependent on the irregularly reticulate ornamentation and addition of successive layers of calcite during the ontogenetic growth." [copied from Chronos database]
Geological Range:
Last occurrence (top): within P. hariaensis zone (66.39-67.30Ma, top in Maastrichtian stage). Data source: [copied from Chronos database]
First occurrence (base): within R. calcarata zone (75.71-76.18Ma, base in Campanian stage). Data source: [copied from Chronos database]
Plot of range and occurrence data:
Character matrix
test outline: | Subtriangular | chamber arrangement: | Biserial | edge view: | Compressed | aperture: | Interiomarginal |
sp chamber shape: | Inflated | coiling axis: | N/A | periphery: | N/A | aperture border: | Thin flange |
umb chbr shape: | Inflated | umbilicus: | N/A | periph margin shape: | Broadly rounded | accessory apertures: | None |
spiral sutures: | Moderately depressed | umb depth: | N/A | wall texture: | Finely costate | shell porosity: | Finely Perforate: 1-2.5µm |
umbilical or test sutures: | Moderately depressed | final-whorl chambers: | 2.0-2.0 | N.B. These characters are used for advanced search. N/A - not applicable |
Cushman, J. A. (1938). Cretaceous species of Guembelina and related genera. Contributions from the Cushman Laboratory for Foraminiferal Research. 14: 2-28. gs V O Georgescu, M. D. (2007b). Taxonomic re-evaluation of the Late Cretaceous serial planktonic foraminifer Gümbelina punctulata Cushman, 1938 and related species. Revista Española de Micropaleontología. 39: 1-14. gs V O Nederbragt, A. J. (1991). Late Cretaceous biostratigraphy and development of Heterohelicidae (planktic foraminifera). Micropaleontology. 37: 329-372. gs Pessagno, E. A. (1967). Upper Cretaceous planktonic foraminifera from the western Gulf Coastal Plain. Palaeontographica Americana. 5: 245-445. gs V O Missing or ambiguous references: Georgescu 2007; References:
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Braunella punctulata compiled by the pforams@mikrotax project team viewed: 27-1-2021
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