Karsella daviesi SCHLAGINTWEIT 2021, comb. nov.
Description
Karsella daviesi (Hofker, 1966) comb. nov.
1941 Orbitolina sp. – Davies, p. 317 (fide Hofker, 1966). 1966 Orbitolina daviesi n. sp. – Hofker, p. 12, pl. 2, figs. 10-14, pl. 3.
1997 Karsella hottingeri n. gen., n. sp. – Sirel, p. 210, pl. 1, figs. 1-10, pl. 2, figs. 1-4.
Non 2005 Karsella sp. – Tentor and Venturini, fig. 8, 9?, 10-12 [Schroedericonus turriculus (Hottinger & Drobne)].
2006 Karsella hottingeri Sirel – Hottinger, fig. 41K-L.
2010 Karsella hottingeri Sirel – Afzal, p. 115, pl. 14, figs. 5-10,?11-13?, 14.
2014 “ Orbitolina ” daviesi J. Hofker jun. – Hottinger, p. 51, pl. 4.9, fig. 2.
2018 Karsella hottingeri Sirel – Cruz-Abad, p. 84, fig. 78A-E (reproduction of Sirel, 1997).
2018 “ Orbitolina ” daviesi Hofker – Cruz-Abad, fig. 78F-H.
2020 Karsella hottingeri Sirel – Schlagintweit, figs. 1, 2A-B (reproductions of Sirel, 1997, Hottinger, 2006, and Afzal, 2010).
Description: Test large, high-conical to slightly cylindroconical with moderately convex base. The megalospheric embryo is situated in a central position at the rounded apex and presents a diameter of up to 0.5 mm. It consists of an irregular ellpisoidal proloculus, a large deuteroconch with partitions (supraembryonic zone) and a few broad peri-embryonic chambers (“subembryonic zone”) that are sporadically subdivided. The neanic stage consists of up to 27 uniserial chambers subdivided into marginal, broad radial, and reduced central zones. There are 5-7 chambers per the last millimeter of the axial cone length. The marginal zone is complex, displaying several orders of beams and rafters. The main partitions (septula), are triangular in axial section, increase in thickeness towards the cone centre and alternate in position between subsequent chambers. In transverse sections, the septula display a zig-zag pattern with associated radially arranged foramina piercing the septa obliquely. The septula form an irregular network displaying oblique stolon axes in the reduced central zone. Wall agglutinated.
Occurrences: Karsella daviesi (Hofker) comb. nov. is known from the Thanetian of Turkey (Sirel, 1997), and Pakistan (Hofker, 1966; Hottinger, 2006; Afzal, 2010).
Notes
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Linked records
Additional details
Identifiers
Biodiversity
- Scientific name authorship
- SCHLAGINTWEIT
- Kingdom
- Chromista
- Phylum
- Foraminifera
- Order
- Loftusiida
- Family
- Orbitolinidae
- Genus
- Karsella
- Species
- daviesi
- Taxon rank
- species
- Taxonomic status
- comb. nov.
- Taxonomic concept label
- Karsella daviesi (SCHLAGINTWEIT, 1966) sec. SCHLAGINTWEIT, 2021
References
- Hofker, J. Jr., 1966. Studies on the family Orbitolinidae. Palaeontographica, Abt. A, 126: 1 - 34.
- Hottinger, L., 2006. Illustrated glossary of terms used in foraminiferal research. Carnets de Geologie / Notebooks on Geology, Memoir 2006 / 02 (CG 2006 _ M 02).
- Afzal, J., 2010. Evolution of Larger Benthic Foraminifera during the Paleocene-Early Eocene interval in the East Tethys (Indus Basin, Pakistan). PhD Thesis University of Leicester: 1 - 291. https: // core. ac. uk / display / 2796424