Praeneodiscus convexus, 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 : 56-58

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/02EC9CA2-153A-4708-AFB6-AAFD3D882787

taxon LSID

lsid:zoobank.org:act:02EC9CA2-153A-4708-AFB6-AAFD3D882787

treatment provided by

Felipe

scientific name

Praeneodiscus convexus
status

gen. nov.

Praeneodiscus convexus View in CoL n. gen. n. sp.

Figures 22.4, 22.7, 22.8, 22.10, 22.12-22.14 View FIGURE 22. 1, 3 , 33.17, 33.22, 33.26 View FIGURE 33. 1-14, 16, 18 , 34.14 View FIGURE 34. 1-5

zoobank.org/ 02EC9CA2-153A-4708-AFB6-AAFD3D882787

? v. 2009 Midiella ? n. sp.; Krainer, Lucas and Vachard, pl. 4, figs. 1, 2, 3.

v. 2013 Midiella ; Brose, Lucas and Krainer, fig. 6.11.

v. 2013 b Neodiscus ? ex gr. ovatus (Grozdilova) ; Vachard, Krainer and Lucas, p. 348 (no illustration).

Etymology. A species with regularly convex flanks.

Holotype. NMMNH P-67606; Figure 22.4 View FIGURE 22. 1, 3 ; sample MG 10-24 .

Paratypes. NMMNH P-67607-67612; Figure 22.7- 8, 22.10, 22.12-14 View FIGURE 22. 1, 3 .

Material. 40 specimens.

Locus Typicus. NMMNH locality 8905; Yeso Group, Los Vallos Formation, Torres Member, Massacre Gap, southern Fra Cristobal Mountains (New Mexico).

Stratum Typicum. Early? Kungurian (late Leonardian).

Diagnosis. Praeneodiscus characterised by an ovoid test, medium to large in diameter, with oscillating coiling and an ogival lumen of the tubular chamber.

Description. Test ovoid. Oscillating involute coiling. No umbilici. No sutures. Wall surface smooth. Lateral sides of spire strongly inflated. Peripheral margin rounded. Proloculus spherical and small to moderate in size, followed by a tubular chamber with a diameter that is equal to the height of the third volution. D = 0.35-0.50-(0.70) mm; w = (0.14)- 0.22-0.35 mm; w/D = 0.50-0.70; whorls: (4)-5-6; p = 0.01-0.02-(0.05-0.06) mm; h = 0.05-0.10 mm; s = 0.01-0.02 mm.

Remarks. The new species differs from Praeneodiscus arcticus n. comb. (formerly Midiella arctica ) by a less sigmoidal coiling and a less inflated test (probably 0.66-0.71 in this latter species; although the ratio D/w indicated by Blazejowski, 2009 is 2.4- 2.5; a probable lapsus calami for 1.4-1.5). It differs from P. compressus ( Lipina, 1949) n. comb. by more whorls and more aligned last whorls. In contrast to P. ovatus ( Grozdilova, 1956) n. comb. which is relatively similar in the shape of the tube lumina (i.e., crescentic, very wide, and well-developed in the lateral sides), the lumina of P. convexus n. gen. n. sp. are smaller, semicircular and limited to the central part of the test; the test, itself, of P. ovatus is much larger with D = 0.490 -0.990 mm; w = 0.340 -0.480 mm (for the same number of whorls: 5-6); h = 0.076 -0.150 mm; s = 0.026 -0.038 mm. Praeneodiscus darvasica n. comb. is similar to P. ovatus ; it differs from P. convexus n. gen. n. sp. by a shorter lumen of the chambers and a glomus more developed by the internal and external whorls. The holotype of P. convexus n. gen. n. sp. ( Figure 19.4 View FIGURE 19. 1-2, 4-6, 9 ) is similar to Neodiscus padangensis sensu Kobayashi (2006 , figures 4, 5), but differs by its smaller size (1.00 mm for the Kobayashi’s specimen), its smaller proloculus, and the total similarity of all lumina, whereas Kobayashi’s specimen seems to exhibit a juvenarium, as does the holotype of N. milliloides Miklukho-Maklay, 1953 or Neodiscus cf. N. milliloides sensu Nestell et al., 2009 (plate 1, figures 30, 31). Praeneodiscus convexus n. gen. n. sp. differs from P. longus n. comb. and P. permicus n. comb. by the more inflated test and therefore a larger width; from Midiella zaninettiae ( Altiner, 1978) by larger dimensions and a more oscillating coiling; from Neodiscus quinqlongensis Wang, 1976 by a test less inflated test with more volutions for a similar diameter; and from Neohemigordius zulumartensis Filimonova, 2010 by larger dimensions.

Occurrence. Early?-middle? Kungurian (late Leonardian) of New Mexico (Yeso Group, Los Vallos Formation, Torres Member: sample MG 10-24; San Andres Formation, McLeod Hills: samples MLY 5-4, MLY(2) 5-5, MLY 5-7, MLY 5-7a, MLY(2) 5-8, MLY 5-8a, MLY(2) 5-8a, MLY 5-9, MLY 5-13, MLY(2) 5-19b, MLY 5-21, MLY 5-30, MLY 5-31, MLY 5-32, MLY(2) 5a-14, MLY(2) 5a-16, MLY(2) 5a-17, MLY(2) 5a-18, MLY 8-1).

NMMNH

New Mexico Museum of Natural History and Science

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