Nodosinelloides longa ( Lipina, 1949 )

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 : 60

publication ID

https://doi.org/ 10.26879/433

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scientific name

Nodosinelloides longa ( Lipina, 1949 )
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Nodosinelloides longa ( Lipina, 1949) View in CoL

Figure 25.6-25.7, 25.10, 25.17-25.19 View FIGURE 25. 1-2

1949 Nodosaria longa Lipina , p. 216-217, pl. 4, fig. 6.

v. 2009 Nodosinelloides longa (Lipina) ; Krainer, Lucas and Vachard, pl. 5, figs. 2, 5, 6; pl. 6, fig. 23.

2010 Nodosinelloides longa (Lipina) ; Filimonova, p. 784, 786, pl. 5, fig. 19 (with synonymy).

v. 2013 Geinitzina ; Brose, Lucas and Krainer, fig. 6.5.

v. 2013 b Nodosinelloides longa (Lipina) ; Vachard, Krainer and Lucas, p. 348 (no illustration).

Description. Test cuneate, rectilinear, slightly curved to curved, very strongly elongate. Chambers subrectangular, fabiform to semicircular. Wall thin, bilayered, with small inner layer. H = 0.24- 0.38-(0.60) mm; w = 0.05-0.09-(0.13) mm; w/H = 0.22-0.50; chambers: 7-12; p = 0.01-0.02-(0.03) mm; h = 0.05-0.09 mm; s = 0.01 mm.

Remarks. Nodosinelloides longa might be characteristic of the early Kungurian according to Sosipatrova (1972) and Pronina (1999). However, it may be present as early as the earliest Permian (Vachard and Krainer, 2001a, 2001b; Krainer et al., 2009; Filimonova, 2010).

Occurrence. Late? Kungurian (latest Leonardian) of New Mexico (San Andres Fm: samples SAR 8a- 4a, SAR 8a-8, SAR 8a-17, SAR 11a-6, SAR 11a-9, SAR 12-4, SAR(2) 12-17).

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