Globivalvulina praegraeca, Vachard, Krainer & Lucas, 2015

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 : 34-36

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/F390F0B9-8701-49DB-A753-F7ECDDC800AB

taxon LSID

lsid:zoobank.org:act:F390F0B9-8701-49DB-A753-F7ECDDC800AB

treatment provided by

Felipe

scientific name

Globivalvulina praegraeca
status

sp. nov.

Globivalvulina praegraeca View in CoL n. sp.

Figures 21.9-21.14 View FIGURE 21. 1-8 , 28.4-28.6, 28.8-28.12, 28.14- 28.16 View FIGURE 28. 1-3, 7 , 29.5, 29.8, 29.10-29.13 View FIGURE 29. 1-4, 7 , 30.1, 30.4-30.6, 30.8-30.10, 30.12, 30.14, 30.15 View FIGURE 30. 1, 4-6, 8-10, 12, 14-15 , 31.2-31.8 View FIGURE 31. 1

zoobank.org/ F390F0B9-8701-49DB-A753-F7ECDDC800AB

1970 Globivalvulina graeca Reichel ; KochanskyDevidé, p. 185, pl. 9, fig. 6; pl. 18, figs. 1,

2. 1972 Globivalvulina aff. donbassica Potievskaya ;

Sosipatrova, pl. 10, figs. 14, 15. 1974 Globivalvulina graeca Reichel ; Akopian, p.

101, pl. 39, fig. 4. 2009 Globivalvulina syzranica Reitlinger ; Blazejowski, fig. 10.3. 2009 Globivalvulina graeca Reichel ; Blazejowski,

figs. 10.4-5. 2009 Globivalvulina cf. graeca Reichel ; Blazejowski, fig. 10.6- 9. v. 2013 b Globivalvulina cf. graeca Reichel ;

Vachard, Krainer and Lucas, p. 348 (no illustration). Etymology. Probable ancestor of G. graeca Reichel, 1946 . Holotype. NMMNH P- 67564; Figure 21.12 View FIGURE 21. 1-8 ; sample SAR 7-7 About SAR . Paratypes. NMMNH P- 67565-67569; Figure 21.9- 11, 21.13-14 View FIGURE 21. 1-8 . Material. 40 specimens. Locus Typicus. NMMNH locality 8900; San Andres Formation, reference section in the San Andres Mountains (New Mexico). Stratum Typicum. Late? Kungurian (latest Leonardian ). Diagnosis. Test large, with a wide aperture, a deep and relatively wide funnel, no oral valvula, and a bilayered wall, but with an inner pseudofibrous layer that is very thin and discontinuous. Description. Test nautiloid, involute, and large: D = (0.45)-0.50-0.73-(0.83) mm, w = 0.50-0.72 mm, w/D = 0.71-1.0. Planispirally coiled axis of biseriality. Proloculus spherical, small (0.02) to large (0.06-0.13 mm), and subprominent. Dorsal side convex, curved to semicircular. Sutures weak to absent. Whorls : 1-1.5. Peripheral margin rounded to slightly angular; lateral sides of spire slightly inflated; umbilicus absent. Chambers rectangular; the last one is rounded trapezoidal; n = 5-7 (rarely 8); h = (rarely 0.13-0.20)- 0.20-0.43 mm. Septa regular, sigmoid, typical of the genus. Ventral side concave to flattened. Aperture broad with a deep and relatively wide funnel. Oral valvula not obvious. Wall bilayered (s = 0.03-0.05 mm) and relatively thick, microgranular with calcareous agglutinate, locally bilayered with an inner pseudofibrous clear layer that is very thin and not obviously continuous .

Comparisons. The new species differs from G. graeca by smaller dimensions (mean diameter of G. graeca = 0.70 mm), less chambers, wider aperture and less developed funnel, larger proloculus, absence of lamella, and thinner and discontinuously located inner pseudofibrous layer. It differs from G. syzranica Reitlinger, 1950 by the shape of the chambers and the deeper funnel; from G. donbassica Potievskaya, 1962 by larger dimensions (in this latter species, D = 0.31-0.42 mm; w = 0.26- 0.39 mm), and higher chambers (maximum 0.22 mm, mainly 0.11-0.15 mm in G. donbassica ), and from G. granulosa Reitlinger, 1950 by the stronger development of the pseudofibrous inner layer, less thick wall (up to 0.06 mm-thick in G. granulosa ), less coarse calcareous agglutinate, and the deep funnel. Furthermore, contrary to Pinard and Mamet (1998), we do not assign G. granulosa to the group G. bulloides , because of the difference of wall microstructure.

Occurrence. Early Permian of Croatia and Armenia. Early Artinskian of Spitsbergen. Middle?-late? Kungurian (late Leonardian) of New Mexico (San Andres Formation, McLeod Hills (MLY) and reference section in the San Andres Mountains (SAR): samples MLY 3-3, MLY(2) 4-9, MLY 6-18, samples SAR 3-4, SAR 7-1, SAR 7-2, SAR 7-4, SAR 7-5, SAR 7-6, SAR 7-7, SAR 8-1, SAR(2) 8-1a, SAR 8- 2, SAR(2) 8-3, SAR(2) 8-4, SAR(2) 8-6, SAR 8-7, SAR 8-7a, SAR(2) 8-8, SAR(2) 8-10, SAR(2) 8-18, SAR(2) 8-21, SAR 8a-2, SAR 8a-5, SAR 8a-10, SAR 8a-10a, SAR 8a-12, SAR 8a-13a, SAR 8a-20, SAR 8a-21, SAR 8a-24, SAR 9-1, SAR 12-7, SAR 13-1, SAR(2) 13-2, SAR(2) 13-6, SAR(2) 13-9, SAR(2) 13a-4).

NMMNH

New Mexico Museum of Natural History and Science

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