Pseudotextulariella cretosa ( Cushman, 1932 )
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 ) |
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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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