Taxonomy
Original description: The delicate asteroid test resembles the Middle Eocene Hantkenina (Aragonella) mexicana Cushman. Only the last five-chambered volution is visible. The chambers are arranged in an indistinct trochoidal spiral. The peripherally well-separated chambers are compressed, except the end chamber, which in some individuals is slightly inflated. The chambers are radially elongate and possess throughout the last whorl axially situated spines. The angles between the spines measure on the average 70 degrees. In general, the spines of the last chambers are smaller than those of the earlier ones. It is possible that this feature becomes obsolete in the course of the ontogenetic development. The umbilicus is indistinct, and the central areas on both sides are masked by matrix. The sutures are straight, shallow but clearly defined. The aperture is not known. The walls appear to be thick. The surface is rugose and, in a few specimens, even a kind of linear pattern can be observed. Due to the indistinct trochoidal spiral the direction of coiling cannot be determined.
Entries in the Catalog of original descriptions: Rugoglobigerina (Plummerella) hantkeninoides hantkeninoides, Rugoglobigerina (Plummerella) hantkeninoides costata, Rugoglobigerina (Plummerella) hantkeninoides inflata
Character matrix
test outline: | Stellate | chamber arrangement: | Trochospiral | edge view: | aperture: | Umbilical | |
sp chamber shape: | Subtriangular | coiling axis: | Very low | periphery: | N/A | aperture border: | Tegilla |
umb chbr shape: | Subtriangular | umbilicus: | Wide | periph margin shape: | Subangular | accessory apertures: | Infralaminal |
spiral sutures: | Moderately depressed | umb depth: | Shallow | wall texture: | Meridional costellae | shell porosity: | |
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. hantkeninoides zone (66.04-66.39Ma, top in Maastrichtian stage). Data source: [copied from Chronos database]
First occurrence (base): within A. mayaroensis zone (67.64-69.27Ma, base in Maastrichtian stage). Data source: [copied from Chronos database]
Plot of range and occurrence data:
Brönnimann, P. (1952c). Globigerinidae from the Upper Cretaceous (Cenomanian-Maestrichtian) of Trinidad, B. W. I. Bulletins of American Paleontology. 34(140): 1-70. gs Robaszynski, F., Caron, M., Gonzales Donoso, J. M., Wonders, A. A. H. & the European Working Group on Planktonic Foraminifera (1984). Atlas of Late Cretaceous globotruncanids. Revue de Micropaléontologie. 26(3-4): 145-305. gsReferences:
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Plummerita hantkeninoides compiled by the pforams@mikrotax project team viewed: 13-2-2025
Short stable page link: https://mikrotax.org/dinotax/index.php?id=110420 Go to Archive.is to create a permanent copy of this page - citation notes |
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