Pseudotextulariella cretosa ( Cushman, 1932 )

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 : 424-425

publication ID

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

persistent identifier

https://treatment.plazi.org/id/0399F83C-FFD2-FFF5-FCD8-9071C98A4900

treatment provided by

Felipe

scientific name

Pseudotextulariella cretosa ( Cushman, 1932 )
status

 

Pseudotextulariella cretosa ( Cushman, 1932) View in CoL

Fig. 8s View Figure 8

1932. Textulariella cretosa Cushman.

1989. Pseudotextulariella cretosa (Cushman) ; Frieg, p. 362, text-figs. 2 a–h, pl. 1, figs. 1–11.

Material

A total of 139 specimens from the Baddeckenstedt section, 1 specimen from the Söhlde section, 5 specimens from the Wunstorf Wu2010/1 core, 35 specimens from the Wunstorf Wu2010/3 core, and 4 specimens from the Wunstorf Wu2010/4 core.

Remarks

This species is used as index fossil for the Cenomanian of the English chalk (Hart et al., 1989), but Frieg (1989) already proved its existence in the lower part of the Albian. Our findings of four specimens in the middle Turonian of Wunstorf extends the stratigraphical range of this species and supports the idea of Frieg (1989) of a facies related appearance of Pseudotextulariella cretosa as it does not appear in the middle Turonian of Söhlde .

Occurrence

Abundant to common in the lower and middle Cenomanian at Baddeckenstedt, rare to very rare in the Cenomanian and Turonian of Wunstorf, and absent in the Turonian of Söhlde.

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