Taxonomy
Original description: Test small, nearly symmetrical, slightly involute, periphery broadly rounded, earlier whorls partly exposed on both sides at the center; chambers inflated, increasng rather rapidly in size as added, quite uniform in shape, numbering 7-9 in last whorl; sutures strongly impressed, usually curving backward as they pass over the periphery; wall conspicuously perforated; aperture peripheral passing onto the dorsal side.
Entries in the Catalog of original descriptions: Anomalina bentonensis, Planomalina caseyi, Globigerinella cushmani
Emended description:
Morphology:
Wall type:
Size:
Most likely ancestor: Laeviella primuloides - at confidence level 3 (out of 5). Data source: Huber et al. 2022.
Likely descendants: Laeviella tururensis; Laeviella bollii;
plot with descendants
Geological Range:
Last occurrence (top): within R. cushmani zone (94.03-95.94Ma, top in Cenomanian stage). Data source: Huber et al. 2022
First occurrence (base): within T. primula zone (107.39-111.84Ma, base in Albian stage). Data source: Huber et al. 2022
Plot of range and occurrence data:
Character matrix
test outline: | Ovate | chamber arrangement: | Planispiral | edge view: | Hourglass | aperture: | Equatorial |
sp chamber shape: | Inflated | coiling axis: | N/A | periphery: | N/A | aperture border: | Thin lip |
umb chbr shape: | Inflated | umbilicus: | Wide | periph margin shape: | Broadly rounded | accessory apertures: | None |
spiral sutures: | Moderately depressed | umb depth: | Shallow | wall texture: | Smooth | shell porosity: | - |
umbilical or test sutures: | Moderately depressed | final-whorl chambers: | 7.0-9.0 | N.B. These characters are used for advanced search. N/A - not applicable |
Eicher, D. L. & Worstell, P. (1970). Lunatriella, a Cretaceous heterohelicid foraminifer from the western interior of the United States. Micropaleontology. 16(1): 117-121. gs Falzoni, F., Petrizzo, M. R., Jenkyns, H. C., Gale, A. S. & Tsikos, H. (2016). Planktonic foraminiferal biostratigraphy and assemblage composition across the Cenomanian–Turonian boundary interval at Clot Chevalier (Vocontian Basin, SE France). Cretaceous Research. 59: 69-97. gs Leckie, M. (1984). Mid-Cretaceous planktonic foraminiferal biostratigraphy off Central Morocco, Deep Sea Drilling Project Leg 79, Sites 545 and 547. Initial Reports of the Deep Sea Drilling Project. 79: 579-620. gs V O Morrow, A. L. (1934). Foraminifera and ostracoda from the Upper Cretaceous of Kansas. Journal of Paleontology. 8: 186-205. gs Pessagno, E. A. (1967). Upper Cretaceous planktonic foraminifera from the western Gulf Coastal Plain. Palaeontographica Americana. 5: 245-445. gs V OReferences:
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Laeviella bentonensis compiled by the pforams@mikrotax project team viewed: 4-7-2022
Short stable page link: https://mikrotax.org/pforams/index.php?id=110122 Go to Archive.is to create a permanent copy of this page - citation notes |
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