Boueina, F. Toula, 1884

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 : 14-16

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-FD56-FFF4-FC1B-F94C3421F882

treatment provided by

Felipe

scientific name

Boueina
status

 

Boueina View in CoL ? crassundia n. sp.

Figures 11.1-11.4, 11.6, 11.7 View FIGURE 11. 1-4, 6-7 , 13.1, 13.2, 13.4, 13.5, 13.8, 13.10 View FIGURE 13. 1, 4-5, 8, 10 , 14.1-14.4, 14.10 View FIGURE 14. 1-4, 10 , 15.1, 15.2, 15.4, 15.7, 15.9 View FIGURE 15. 1-2, 4, 7, 9 , 16.1, 16.2, 16.6, 16.8 View FIGURE 16. 1-2, 6, 8 , 18.6-18.11 View FIGURE 18. 1-5 , 20.13, 20.15 View FIGURE 20. 1-4

zoobank.org/ F99005B2-1230-43E7-992C-18910EB11B9A

v. 2013 Paraboueina; Brose, Lucas and Krainer, fig. 6.8.

v. 2013 b Boueina ? sp. 2; Vachard, Krainer and Lucas, p. 348 (no illustration).

Etymology. Latin crassundia: large intestine; because of the broad medullar siphons.

Holotype. NMMNH P-67506; Figure 11.1 View FIGURE 11. 1-4, 6-7 ; sample MLY (2) 6-7a.

Paratypes. NMMNH P-67494, 67495, 67496, 67507, 67508; Figure 11.2-4, 11.6-7 View FIGURE 11. 1-4, 6-7 .

Material. 200 specimens.

Locus Typicus. NMMNH locality 8892; San Andres Formation, McLeod Hills (New Mexico).

Stratum Typicum. Middle? Kungurian (late Leonardian).

Diagnosis. Boueina ? with broad siphons in both medullar and cortical zones.

Description. The thallus is cylindrical (L = 1.00- 1.75 mm; w = 0.45-0.75 mm). Medullar zone with medium-sized, tangled, longitudinal threads exhibiting long segments of tubes with a diameter of 0.05-0.09 mm. Cortical zone with relatively wide (0.03-0.04 mm), oblique, and one time branching, radial or oblique threads. The subdermal zone shows some small deltoid terminations (0.03-0.05 mm).

Comparison. Boueina ? crassundia n. sp. differs from B.? tubulata n. sp. by broader siphons, even where the other dimensions are the same. This character is not diagenetic because there are no transitional measurements.

Occurrence. Early?-middle? Kungurian (late Leonardian) of New Mexico (Yeso Group, Los Vallos Formation, Torres Member: samples MG 10-1, MG 10-10, MG(2) 12-6, MG(2) 12-11, MG(2) 12- 15; San Andres Formation, McLeod Hills (lower part); samples MLY 5-1, MLY 5-2, MLY 5-6, MLY(2) 5-6, MLY 5-7b, MLY(2) 5-9, MLY(2) 5-11, MLY(2) 5- 14, MLY(2) 5-16, MLY 5-18, MLY(2) 5-18, MLY(2) 5-19, MLY(2) 5-19d, MLY 5-20, MLY 5-26, MLY 5- 27, MLY 5-28, MLY(2) 5a-1, MLY(2) 5a-3, MLY(2) 5a-4, MLY(2) 5a-10, MLY(2) 5a-11, MLY(2) 5a-12, MLY(2) 5a-13, MLY(2) 5a-19, MLY(2) 5a-19a, MLY(2) 5a-21, MLY(2) 5a-23, MLY(2) 5a-25, MLY(2) 6-7, MLY(2) 6-7a, MLY 6-8, MLY(2) 6-8, MLY(2) 6-8a, MLY 6-10, MLY(2) 6-11, MLY 6-13, MLY 6-14, MLY(2) 6-15, MLY(2) 6-16, MLY(2) 6-17, MLY(2) 6-21, MLY(2) 6-27, MLY(2) 6-28, MLY(2) 6- 30, MLY 8-3)).

NMMNH

New Mexico Museum of Natural History and Science

MLY

Arborétum Mlynany

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