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 />
nilla limestone which forms the cliffs on the<br />
northwest si<strong>de</strong> of a northeast-flowing tributary<br />
of the Rio <strong>de</strong> Santo Domingo about 3<br />
miles south (and possible somewhat east)<br />
of Paseo Hondo", región <strong>de</strong> C'hicomuselo,<br />
Chiapas. "It is associated with Schwagerina<br />
sp. B and Schwagerina sp. G, . . " (Thompson,<br />
M. L. y A. K. Miller, 1944, 500-501,<br />
láms. 80, figs. 1-2 y 82, figs. 5-6) "Paraschwagerina<br />
roveloi Thompson y Miller, n.<br />
sp."<br />
Horizonte geológico: caliza La Vainilla, <strong>de</strong>l<br />
Pérmico Inferior (entre las series Wolfcamp<br />
y Leonard <strong>de</strong> Texas).<br />
Gén. Paleofusulina Deprat, 1913<br />
17) Paleofusulina cf. P. pseudo-prisca Colani<br />
Localidad:<br />
".. .al sur <strong>de</strong> Chicomtiselo, Chiapas" (Mullerried,<br />
F. K. G., 1936, 35) "Fusulina cf.<br />
psewlo-prisca cm Colani (Paleofusulina prisco<br />
Deprat)" "...en cl sur <strong>de</strong> Chiapas"<br />
(Mullerried, F. K. G., 1945, 6) '•Fusulina<br />
cf. pseiuio-prisca era Colani (Paleojusidinnprisca<br />
Deprat)".<br />
Horizonte geológico: Pérmico (¿serie Leonard<br />
<strong>de</strong> Texas?)<br />
Gén. Parafusulina Dunbar y Skinner, 1931<br />
18) Parafusulina australis Thompson y Miller<br />
Localidad!<br />
"...in a medium-gray massive limestone<br />
that occurs in the lower portion of the Paseo<br />
Hondo formation of southern Chiapas<br />
... in the southwest valley wall of a northeast-flowing<br />
tributary of the Rio Santo Domingo<br />
about 3 H miles south (and possibly<br />
somewhat east) of Paseo Hondo" (Thompson,<br />
M. L. y A. K. Miller, 1944, 503, lain.<br />
81, figs. 2-9) "Parafusulina australis<br />
Thompson y Miller, n. sp."<br />
Horizonte geológico: formación Paseo Hondo,<br />
<strong>de</strong>l Pérmico Inferior (serie Leonard <strong>de</strong><br />
Texas).<br />
19) Parafusulina bósei Dunbar y Skinner<br />
Localidad:<br />
".. .abundant in the limestone of bed 6 of<br />
the Malascachas section at locality 41 (fusulinc<br />
limestone <strong>10</strong>00 meters S 17° W of<br />
summit of Cerro Colorado, d'après King,<br />
1944, 33), which is about 4 kilometers SSE.<br />
of Noria <strong>de</strong> Malascachas", región <strong>de</strong> Las<br />
Delicias, Coahuila (Dunbar, C. 0., 1944,<br />
42-43, Iám. 12, figs. 1-9) "Parafusidina bösei<br />
Dunbar y Skinner"<br />
24 ¡r.<br />
Ilorizonte geologieo: Pémiico <strong>Superior</strong> (série<br />
Guadalupe dc Texas)<br />
201 Parafusulina drliciasensis Dunbar y Skinner<br />
Loealidad:<br />
"Very abundant ... in beds 11 to 17 in<br />
the Diftinta section, localities 3 (fusuline<br />
limestone 125 meters S 70° E. of summit<br />
of Cerro Agujito, d'après King, 1944, 31),<br />
7 (concretionary shale <strong>10</strong>00 meters S 23°<br />
E of Cerro Prieto Norte, d'après King, 1944,<br />
31), 12 (alternating shale and graywacke 60<br />
meters N 35° E of La Difunta, d'après King,<br />
1944, 31), 17 (limestone layer 3500 to 4300<br />
meters N 15° E of La Difunta, d'après King,<br />
1944, 32), 23 (fusuline limestone 1400 meters<br />
S 65° W of Cerro Pichagililla, d'après<br />
King, 1944, 32), where it is commonly associated<br />
with Rauserella erratica. In the<br />
Malascachas section it was only found at<br />
locality 2(i (fusuline limestone 600 meters<br />
S 75° W of Noria <strong>de</strong> Malascachas, d'après<br />
King, 1944, 32) where it is associated with<br />
Parafusulina sellardsi", regién <strong>de</strong> Las Delicias,<br />
Coahuila (Dunbar, C. ()., 1944, 42-<br />
43, lain. 12, figs. 1-9) "Parafusulina <strong>de</strong>liciasensis<br />
Dunbar y Skinner."<br />
Ilorizonte geologieo: Pérmico <strong>Superior</strong> (série<br />
Guadalupe <strong>de</strong> Texas).<br />
21) Parafusidina imlayi Dunbar<br />
Loealidad:<br />
"Abundant in a zone about <strong>10</strong>0 feet below<br />
the top of the highest limestone knob at<br />
the south end of Sierra <strong>de</strong> Huachita Hueca,<br />
about 7 miles northeast of Bavispe, Sonora"<br />
(Dunbar, C. O., 1939, 1748-1749, lâm.<br />
1, figs. 1-5) "Parafusidina imlayi Dunbar,<br />
n. sp."<br />
Ilorizonte geologieo: Pérmico Inferior (série<br />
I/îonard <strong>de</strong> Texas).<br />
22) Parafusulina rothi Dunbar y Skinner<br />
I.( >ca ! i ( la ( I :<br />
".. .abundant in the limestone of bed 6 of<br />
the Malascachas section at locality 41 (fusuline<br />
limestone <strong>10</strong>00 meters S 17° W of<br />
summit of Cerro Colorado, d'après King,<br />
1944, 33), which' is about 4 kilometers SSE<br />
of Noria <strong>de</strong> Malascachas", region <strong>de</strong> Las<br />
Delicias, Coahuila (Dunbar, C. O., 1944,<br />
42-43, lain. 12, figs. 1-9) "Parafusulina rothi<br />
Dunbar y Skinner".<br />
Horizonte geolégico: Pérmico <strong>Superior</strong> (série<br />
Guadalupe <strong>de</strong> Texas).