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Números 9-10 - Consejo Superior de Investigaciones Científicas

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CIENCIA<br />

argillaceous limestone. . . exposed along the<br />

trail at the divi<strong>de</strong> on the southeast si<strong>de</strong> of<br />

a northeast-flowing tributary of the Rio <strong>de</strong><br />

Santo Domingo about '¿Y¿ miles south (and<br />

possibly somewhat east) of Paseo Hondo,<br />

Chiapas.. . in association with. . . Sankinella<br />

? sp. and Schwagerina ? sp." (Thompson,<br />

M. L. y A. K. Miller, 1944, 491-492,<br />

lam. 80, figs. 7-11) "Stajfella centralis<br />

Thompson y Miller."<br />

Horizonte geológico: formación Paseo Hondo,<br />

<strong>de</strong>l Pérmico Inferior (serie Leonard <strong>de</strong> Texas).<br />

3) Staffella fouiUaini Dunbar y Skinner<br />

Localidad:<br />

".. .at localities 29 (limestone layer 2 400<br />

meters S 2° W of Cerro Pichagüilla, d'après<br />

King, 1944, 32) and 30 (limestone layer<br />

2 000 m S 47° W of Noria <strong>de</strong> Malascachas,<br />

d'après King, 1944, 32)", región <strong>de</strong> Las Delicias,<br />

Coahuila (Dunbar, C. O., 1944, 38-<br />

39, lftms. 9, figs. 9-15 y <strong>10</strong>, fig. 16) "Staffella<br />

fountaini Dunbar y Skinner".<br />

Horizonte geológico: Pérmico <strong>Superior</strong> (serie<br />

Guadalupe <strong>de</strong> Texas).<br />

4) Staffella subacula Dunbar<br />

Localidad:<br />

"In great abundance in certain layers of<br />

bed 17 of the Difunta section at locality 12<br />

(alternating shale and graywacke 60 meters<br />

N 35° E of La Difunta, d'après King, 1944,<br />

31), where it is associated with Parafustdina<br />

<strong>de</strong>liciasensis", región <strong>de</strong> Las Delicias, Coahuila<br />

(Dunbar, C. O., 1944, 39-40, lama. <strong>10</strong>,<br />

figs. 8-15 y 11, fig. 1) "SUiffella subacula<br />

Dunbar, n. sp."<br />

Horizonte geológico: Pérmico <strong>Superior</strong> (serie<br />

Guadalupe <strong>de</strong> Texas).<br />

Gén. Rauserella Dunbar, 1944<br />

5) Rauserella errática Dunbar<br />

Localidad :<br />

".. .at localities 3 (fusuline limestone 125<br />

meters S 70° E of summit of Cerro Agujito,<br />

d'après King, 1944, 31) and 20 (along strike<br />

from Cerro Wenceslao on south to 300 meters<br />

west of El Indio on north, d'après King,<br />

1944, 32)", región <strong>de</strong> Las Delicias, Coahuila<br />

(Dunbar, C. O., 1944, 37-38, lám. 9, figs.<br />

1-8) "Rauserella errática Dunbar, n. sp."<br />

Horizonte geológico: Pérmico <strong>Superior</strong> (serie<br />

Guadalupe <strong>de</strong> Texas).<br />

Gén. Schubertella Staff y We<strong>de</strong>kind, 19<strong>10</strong><br />

6) Schubertella mullerriedi Thompson y Miller<br />

243<br />

Localidad;<br />

"extremely abundant in a massive limestone.<br />

.. in the Paseo Hondo formation of<br />

Chiapas. . exposed well up in the bluff on<br />

the south si<strong>de</strong> of the north trail between<br />

Portales and Paseo Hondo abouth 31^ miles<br />

east of Portales and just west of the eastern<br />

of the two passes between Portales and Paseo<br />

Hondo... in association with... Schwagerina<br />

sp. A", región <strong>de</strong> Chicomuselo, Chiapas<br />

(Thompson, M. L. y A. K. Miller, 1944,<br />

488-489, lám. 79, figs. 5-11) "Schubertella<br />

mullerriedi Thompson and Miller, n. sp."<br />

Horizonte geológico: formación Paseo Hondo,<br />

<strong>de</strong>l Pérmico Inferior (serie Leonard <strong>de</strong> Texas).<br />

Gén. Triticites Girty, 1904<br />

7) Triticites piloncillensis Dunbar<br />

Localidad:<br />

"Abundant in the limestone exposed at Los<br />

Piloncillos, locality 27 (fusuline-crinoidal<br />

limestone at northeast point of main hill,<br />

d'après King, 1944, 32) (and probably at<br />

El Fraile)", región <strong>de</strong> Las Delicias, Coahuila<br />

(Dunbar, C. O., 1944, 40-41, lám. <strong>10</strong>,<br />

figs. 1-7) "Triticites piloncillensis Dunbar,<br />

n. sp."<br />

Horizonte geológico: Pennsilvánico superior<br />

(más arriba <strong>de</strong> la serie Des Moines <strong>de</strong>l Pennsilvánico<br />

<strong>Superior</strong> y más abajo <strong>de</strong> la serie<br />

Leonard <strong>de</strong>l Pérmico <strong>de</strong> Texas).<br />

8) Triticites sp. A Dunbar<br />

Localidad:<br />

".. .300 feet below the highest exposure of<br />

the Paleozoic limestone in the section at<br />

the south end of Sierra <strong>de</strong> Huachita Hueca.<br />

Associated with Triticites sp. B", al SSE <strong>de</strong><br />

Agua Prieta, Sonora (Dunbar, C. O., 19396,<br />

1752, lain. 4, figs. 1 y 2A) "Triticites Bp. A".<br />

Horizonte geológico: Pennsilvánico <strong>Superior</strong><br />

(grape Cisco <strong>de</strong> Texas).<br />

9) Triticites sp. B Dunbar<br />

Localidad:<br />

"Associated with Triticites sp. A... about<br />

300 feet below the highest exposures of the<br />

Paleozoic limestone in the section at the<br />

south erid of Sierra <strong>de</strong> Huachita Hueca", la<br />

SSE <strong>de</strong> Agua Prieta, Sonora (Dunbar, C.<br />

O., 1939, 1752, lám. 4, fig. 2B) "Triticites<br />

sp. B".<br />

Horizonte geológico: Pennsilvánico <strong>Superior</strong><br />

(grupo Cisco <strong>de</strong> Texas)..

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