Globotruncanella saratogensis (Applin 1920)

Neagu, Theodor, 2016, Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera, Acta Palaeontologica Romaniae 12 (2), pp. 67-91 : 74

publication ID

https://doi.org/ 10.5281/zenodo.13190456

DOI

https://doi.org/10.5281/zenodo.13190265

persistent identifier

https://treatment.plazi.org/id/D647B844-2F08-4415-FF46-C364FE40F9CF

treatment provided by

Felipe

scientific name

Globotruncanella saratogensis (Applin 1920)
status

 

Globotruncanella saratogensis (Applin 1920)

Figs 3 View Fig : 25-27; Figs. 7 View Fig : 16-18

1920 Globigerina cretacea d'Orbigny var. saratogensis Applin , p. 98, pl.3, fig.8.

Dimensions: D = 0,43-0,46 mm; d = 0,36- 0,36 mm; g = 0,19 mm

Remarks: In the paper of Applin et al. (1925) in the last part of this article were described few species of foraminifera. Some of these species belong to the Paleogen, but there are also two species from the Upper Cretaceous: Globigerina marginata d'Orbigny and a new taxon Globigerina cretacea var. saratogensis ( Fig. 17 View Fig : 1-6 in the present paper). In the description of this new subspecies, Applin et al. (1925, p. 98) pointed out the following features: " chambers increasing gradually in size, sometime slightly carinated at the periphery (which is frail represented on the figure) wall smoothing. The regularity of coiling and the tendency for the form to develop a carinared rim.".......Taking in consideration all the presented features, our specimens ( Fig. 3 View Fig : 25-27) corresponds with the Applin taxon.

By the inflated character of the chambers, spiral and umbilical, this species differs from Bolli's Praeglobotruncana coarctata 1957.

Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian.

Specimens: LPB.IV. 12441

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