Números 9-10 - Consejo Superior de Investigaciones Científicas
Números 9-10 - Consejo Superior de Investigaciones Científicas
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)..