Geinitzina indepressa Cherdyntsev, 1914

Vachard, D, Krainer, K & Lucas, SG, 2015, Late Early Permian (late Leonardian; Kungurian) algae, microproblematica, and smaller foraminifers from the Yeso Group and San Andres Formation (New Mexico; USA), Palaeontologia Electronica (English ed.) 3 (8), pp. 1-77 : 62

publication ID

https://doi.org/ 10.26879/433

publication LSID

lsid:zoobank.org:pub:76D74301-4F2F-4A01-ADE5-EF52F8B53659

persistent identifier

https://treatment.plazi.org/id/03F9582F-FD66-FFC6-FCB6-FF51363CFA3F

treatment provided by

Felipe

scientific name

Geinitzina indepressa Cherdyntsev, 1914
status

 

Geinitzina indepressa Cherdyntsev, 1914 View in CoL

Figure 25.8-25.9, 25.12-25.14 View FIGURE 25. 1-2

1914 Geinitzina indepressa Cherdyntsev , p. 26-27, pl. 1, fig. 9.

2000 Geinitzina indepressa Cherdyntsev ; Groves, p. 300-301, pl. 5, figs. 1, 2, 3, 4, 5, 6 (with synonymy).

v. 2013 b Geinitzina ex gr. postcarbonica Spandel - Vachard, Krainer and Lucas, p. 348 (no illustration).

Description. Test straight triangular, moderately elongate. Chambers semisinushaped. H = (0.14)- 0.16-0.45 mm; w = (0.07)- 0.10-0.22 mm; h = (0.02)- 0.03-0.06 mm; s = 0.01 mm. Proloculus spherical, a little prominent, 0.02-0.03 mm in diameter. Up to nine chambers, relatively short and high for the genus; moreover, the central depression is absent or very faint. Aperture terminal, central, simple, a little depressed.

Remarks. This species differs from G. postcarbonica in the shape of the chambers with a convex roof and not a centrally depressed one, and from G. spandeli plana Lipina, 1949 , which is relatively similar, by more chambers and a smaller proloculus.

The material of Groves (2000) is remarkably similar to ours and proves the importance of this species for the stratigraphic and geographic correlations in North America.

Occurrence. Early Permian (sensu lato) of Russian Platform, Urals, and Xizang ( China). Artinskian (early Leonardian) of Oklahoma ( USA). Late? Kungurian (late Leonardian) of New Mexico (San Andres Fm: samples SAR 8a-7, SAR 8a-11, SAR 8a-14, SAR(2) 11-2, SAR 11-13, SAR 11a-10, SAR(2) 13-7, SAR(2) 13-10, SAR 18-1, SAR(2) 19- 11).

Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF