Vialovella frankei ( Cushman, 1936 )

Besen, Richard M., Struck, Ulrich & Seibertz, Ekbert, 2021, Albian to Turonian agglutinated foraminiferal assemblages of the Lower Saxony Cretaceous sub-basins - implications for sequence stratigraphy and paleoenvironmental interpretation, Fossil Record 24 (2), pp. 395-441 : 420-421

publication ID

https://doi.org/ 10.5194/fr-24-395-2021

persistent identifier

https://treatment.plazi.org/id/0399F83C-FFD6-FFF1-FCD8-9156CA754B0B

treatment provided by

Felipe

scientific name

Vialovella frankei ( Cushman, 1936 )
status

 

Vialovella frankei ( Cushman, 1936) View in CoL

Fig. 8j View Figure 8

1936. Arenobulimina frankei Cushman , p. 27, pl. 4, figs. 5ab.

1969. Arenobulimina frankei Cushman ; Gawor-Biedowa, p. 84, pl. 5, figs. 4, 5, pl. 7, figs. 6–8.

1972. Vialovella frankei (Cushman) ; Voloshina, p. 87, pl. 8, fig. 8.

1977. Arenobulimina frankei Cushman ; Carter and Hart, p. 15, pl. 1, fig. 1, pl. 2, fig. 5.

1982. Vialovella praefrankei (Cushman) ; Frieg and Price, p. 47, pl. 2.1., figs. a–c.

1989. Vialovella frankei (Cushman) ; Frieg and Kemper, p. 104, pl. 15, figs. 12–20.

Material

A total of 443 specimens from the Baddeckenstedt section, 38 specimens from the Söhlde section, 297 specimens from the Wunstorf Wu2010/1 core, 269 specimens from the Wunstorf Wu2010/3 core, and 19 specimens from the Wunstorf Wu2010/4 core.

Remarks

Initially described as Arenobulimina frankei by Cushman (1936), Frieg and Price (1982), and Frieg and Kemper (1989) described the clearly triserial chamber arrangement of this species. Therefore, we follow their classification as Vialovella frankei .

Occurrence

Very abundant to common in the uppermost Albian up to the upper Cenomanian. Last occurrence below the Facies Change at Söhlde and Baddeckenstedt and in the plenus Bed at Wunstorf.

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